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Updated: Jul 18, 2026

Preparing an Isotopically Pure 229Th Ion Beam for Studies of 229mTh
10:42

Preparing an Isotopically Pure 229Th Ion Beam for Studies of 229mTh

Published on: May 3, 2019

トンガ・ケルメデック島の下の融解の動態は,231Pa−235U体系から推論された

Bourdon1, Turner, Allegre

  • 1Laboratoire de Geochimie et Cosmochimie, Institut de Physique du Globe de Paris-CNRS, UMR7579, 4 Place Jussieu, 75252 Paris Cedex 05, France. Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA, UK.

Science (New York, N.Y.)
|January 5, 2000
PubMed
まとめ

トンガ・ケルマデック・ラバのプロタクトニウム231とウラン235の比率を研究すると,流体添加と部分的な溶融の歴史が明らかになる. トンガの溶岩は6万年前の流体添加を示し,ケルメデックの溶岩は溶融効果が過剰に印刷されていることを示している.

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